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Information Journal Paper

Title

Saheb Granitoid Batholith, North of Kurdistan: An Evidence of Cretaceous-Paleocene Magmatism in the Sanandaj-Sirjan Zone

Pages

  33-34

Abstract

 Introduction: The Iranian plateau is part of the Alpine-Himalayan orogenic belt, which consists of several continental fragments separated from each other by major boundary faults and/or ophiolitic suture zones (Gansser, 1981). Generally, the tectonic evolution of Iran has been controlled by the opening and closure of the Proto-Tethys, Paleo-Tethys and the Neo-Tethys during the Precambrian-Cambrian, Paleozoic and Cenozoic, respectively. The study area is located in the northwest of Iran (the Kurdistan province) and 20 km northeast of the city of Saqez. This area is a part of the northern Sanandaj-Sirjan Zone (Aghanabati, 2005). This belt is response to opening and subduction of Neo-Tethyan oceanic crust beneath the Central Iran (Alavi, 1994). During Cretaceous-Tertiary eras, numerous Granitoid bodies were formed in this belt...

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    APA: Copy

    Abdollahi, Farideh, NABATIAN, GHASEM, Li, Jian Wei, HONARMAND, MARYAM, & EBRAHIMI, MOHAMMAD. (2020). Saheb Granitoid Batholith, North of Kurdistan: An Evidence of Cretaceous-Paleocene Magmatism in the Sanandaj-Sirjan Zone. JOURNAL OF ECONOMIC GEOLOGY, 12(3 (26) ), 33-34. SID. https://sid.ir/paper/365394/en

    Vancouver: Copy

    Abdollahi Farideh, NABATIAN GHASEM, Li Jian Wei, HONARMAND MARYAM, EBRAHIMI MOHAMMAD. Saheb Granitoid Batholith, North of Kurdistan: An Evidence of Cretaceous-Paleocene Magmatism in the Sanandaj-Sirjan Zone. JOURNAL OF ECONOMIC GEOLOGY[Internet]. 2020;12(3 (26) ):33-34. Available from: https://sid.ir/paper/365394/en

    IEEE: Copy

    Farideh Abdollahi, GHASEM NABATIAN, Jian Wei Li, MARYAM HONARMAND, and MOHAMMAD EBRAHIMI, “Saheb Granitoid Batholith, North of Kurdistan: An Evidence of Cretaceous-Paleocene Magmatism in the Sanandaj-Sirjan Zone,” JOURNAL OF ECONOMIC GEOLOGY, vol. 12, no. 3 (26) , pp. 33–34, 2020, [Online]. Available: https://sid.ir/paper/365394/en

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